Radiative imbalance with the sky → Electrical work
Radiative imbalance with the skyRadiative sky coolingTemperature gradientMarangoni effectPressure gradientStreaming potentialIonic currentElectrical work
Epistemic state of the route
- known constituent relations
- 6 / 7 established or replicated · weakest constituent theoretically predicted
- constituent maturity floor
- K3 · theoretically quantified
- search for this exact route
- Not assessed — complete composition not searched.
- recorded-pathway overlap
- shares its closing relations with Electrokinetic microchannel generator · 3/7 relations shared
- route-level evidence
- 0 sources for the complete composition · 11 cited by the constituent steps
- boundaries and interfaces
- BOUNDARY compatible · no region transition
Explorematrix context · physics checks · steps · route evidence · constituent evidence · cite
Matrix context
D = disequilibrium row · C = coupling family column. A cell reads the state of the atlas for that pair.
D.12 × C.20 · Radiative imbalance with the sky × Photothermalfamily: PhotothermalD.12 × C.34 · Radiative imbalance with the sky × Marangonifamily: MarangoniD.12 × C.23 · Radiative imbalance with the sky × Electrokineticfamily: Electrokinetic
Typed bounds on this route
Every limit the atlas holds for this route, as constraint records: reached through bounded_by claims on the route's own entities. Hard bounds (an upper bound or a formula) decide the thermodynamic-bound check above; benchmarks, constitutive relations and resource limits are listed and never decisive. No prose limit exists anywhere (pass 42).
- Radiative cooling power bound · resource-bound · listed, never decisivenet cooling power ≲ 100–150 W/m² under a clear sky
- Carnot limit · formula-bound · hard, applies to this routeη ≤ 1 − T_c/T_h for any heat engine between reservoirs at T_h and T_c
- Onsager–Casimir reciprocity · constitutive-relation · listed, never decisiveL_ij(B) = ε_i ε_j L_ji(−B): the cross-coefficients of coupled linear transport are equal up to the time-reversal parities ε of the variables and reversal of the magnetic field; L_ij = L_ji is the zero-field, even-parity case
Steps
- 01radiative → thermal
- an emitter with high emissivity in the 8–13 µm window and high solar reflectance
- a clear sky; humidity and cloud close the window
refs [1] [2] [3] - 02thermal → thermal
- the cooled surface sits a few kelvin below ambient air
refs [1] [4] [3] - 03thermal → kinetic · loss to thermal
- thermocapillary case: surface tension falls with temperature, so a temperature gradient along the interface drives flow toward the cold side
liquid · temperature gradient requiredrefs [5] [6] - 04kinetic → mechanical · loss to thermal
- a thermocapillary-driven liquid plug moves in a closed-ended microchannel and compresses the trapped gas; the pressure rise is the load presented to the compliant membrane
Kept below demonstrated: the Odukoya device measured heater and droplet behaviour, while the pressure field feeding the membrane (about 0.1 kPa for a 13 μm deflection in the model) comes from the force balance, not a measurement.refs [7] [8] - 05mechanical → electrical · loss to thermal
- electrolyte forced through a channel with charged walls; efficiency peaks when the Debye length is comparable to the channel width
aqueous medium required · bulk flow requiredrefs [9] [10] - 06electrical → electricalrefs [9] [10]
- 07electrical → electrical · loss to thermal
- electrodes exchange the ionic current for an electronic current through the external load
refs [11]
Evidence for the complete composition · 0
No source on record for this exact composition. The sources below support the individual steps, not the route as a whole.
Evidence for the constituent relations · 11
- [1]A. P. Raman et al.. Passive radiative cooling below ambient air temperature under direct sunlight (2014)
- [2]Y. Zhai et al.. Scalable-manufactured randomized glass-polymer hybrid metamaterial for daytime radiative cooling (2017)
- [3]J.-l. Kou et al.. Daytime radiative cooling using near-black infrared emitters (2017)
- [4]A. P. Raman, W. Li, S. Fan. Generating light from darkness (2019)
- [5]L. E. Scriven, C. V. Sternling. The Marangoni Effects (1960)
- [6]Q. Dai et al.. Directional interfacial motion of liquids: Fundamentals, evaluations, and manipulation strategies (2021)
- [7]P. S. Glockner, G. F. Naterer. Surface tension and frictional resistance of thermocapillary pumping in a closed microchannel (2006)
- [8]A. Odukoya, G. F. Naterer. Transient response of thermocapillary pumping of a droplet in a micro heat engine (2013)
- [9]J. Yang et al.. Electrokinetic microchannel battery by means of electrokinetic and microfluidic phenomena (2003)
- [10]R. J. Hunter. Zeta Potential in Colloid Science: Principles and Applications (1981)
- [11]A. J. Bard, L. R. Faulkner. Electrochemical Methods: Fundamentals and Applications (2nd ed.) (2001)
Cite this route
Physical Transformation Atlas (2026). route p-29a721b48d: Radiative imbalance with the sky → Radiative sky cooling → Temperature gradient → Marangoni effect → Pressure gradient → Streaming potential → Ionic current → Electrical work. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/29a721b48d
Ids and matrix addresses are stable across revisions; the revision hash identifies the exact canonical files the record was compiled from and is meta.data_hash in every /api export. Reuse terms: see the license field in any export.